Where does the origin of the Volga takes. Where does the beginning of the Volga, where is it source? In Volzheerhovye! Economic role of the river in the life of the country

The source of the Volga is amazing beautiful placenot touched by modern civilization. Here the time seemed to froze, afraid to disturb and destroy the eternal atmosphere of grace, reigning around. The Volga takes her beginning near the village of Volkheerhovye at the Valdai Hills in the Tver region.

Where is the source of the Volga

You can get to Volkheerhichia from the city of Ostashkov first on a fairly broken track to the village of Svabuchka (about 50 km), and from there on the primer, the state of which is much better than that of the asphalt fabric. From the sampness to the destination of 19 km. Buses in Volzerhovye do not go, so you can only get there on a personal car (geographic coordinates: 57 ° 15`07` 02`2e`2).

The source of the Volga on the map:

From afar long flow river Volga ...

Volgoverhhoid village is located on a low hill, and under the hill from a small swamp originates the great Russian river - Volga.

In this swamp there are several springs. One of them, the deepest, which immediately appears the current, and was defined as the source of the Volga in the middle of the 18th century. A chapel is now built over this spring, to which wooden walkways lead. In the chance itself there is a font where you can plunge directly to the source. The depth here is small: an adult man on his shoulders.

In 1989, a memorable stone was installed in 1989, which says: "Traveler! Rapid on the Volga source! Here the purity and greatness of the land of Russian are born. Here are the origins of the People's Soul. Keep them. Look out the leaving. " This place is located at an altitude of 228 meters above sea level.

The Volga swamp flows out of a small stream, the width of only about 50 cm and a depth of 25-30 cm. Water in just "born" river brown color Because of the peat contained in it, but clean and transparent. There is a bucket on the bedding, so if you wish, you can wash the Volga water or gain it into the bottles and take it with you.

300 meters from the source through the handle, the small bridge is thrown away and there is a convenient descent to the stream, so that in the Volga water can be melted. However, water here even in the heat of the cold, not higher than 15 °.

Olgin Monastery

Next to the bridge, the remains of the stone dam, built by Olgin women's monastery At the beginning of the last century. The dam is now destroyed, and the monastery itself exists in Volzheerhovye until now. IN soviet time He was closed, but revived in 1999 again.

Everything that has survived from the monastery to our time is the Savior-Preobrazhensky Cathedral and the Wooden Church of Nicholas Wonderworker. Services here are held regularly. We fell just on the church holiday - the day of St. Olga. At this time, a congestion took place around the monastery, in which the people for such wilderness were quite a lot: about 150 people.

Since the residential buildings of the monastery are not preserved, the nuns live in the village, their homes are easily recognizable in the roofs on the roofs.

Church of Nicholas Wonderworker

For a small fee, you can climb the bell tower of the Transfiguration Cathedral and take a look at the height of the Iston of the Volga (we didn't get, because because of the holiday, the entrance was temporarily closed).

In the forest, growing around the source of the Volga can be wanted. The paths leading in different directions here are a great set. A multi-voiced bird singing is heard around, butterflies and dragonfly fly.

There is in Volzheerhovye, as in any tourist destination, a small bazaarchik, where they sell ordinary souvenirs, cakes and honey. Cellular communication in these places is absent, it appears only when traveling to the sampling route. Here, despite the fact that the source of the Volga is visited quite a lot of tourists, silence reigns and rest.

After 3 km from its origin, the Volga crosses the dirt road, according to which we went here. This is no longer a stream, but a small river with picturesque shores, overgrown forest.

Volga river The largest I. full-water river Europe. Ancient name RA (lat. RHA) The less old name of the sobs - ITIL, the river received in the Middle Ages. This is the biggest river without falling into the sea. In the Pool Volga lives 2/3 of the population of Russia. Its source is located on the Valdai hill at an altitude of 256 m above sea level. And in the mouth, on the northern coast of the Caspian Sea, in its delta there are the greatest lotus fields in the world that occupy hundreds of hectares.

This is what I wrote about Volga Alexander Duma: "Each country has its own national river. Russia has a Volga - the most large river In Europe, the queen of our rivers, - and I hurried to worship her majesty River Volga! "
River length: 3,530 kilometers.
Waterguide pool area: 1 360 thousand square meters. km.

The highest point: Mount Unnamed, 381.2 m (Zhigulevsky Mountains).

River width: up to 2500 m.

Blope and fall: 256 m and 0.07 m / km (or ppm), respectively.

Average flow rate: less than 1 m / s.

River depth: The middle depth of 8 is 11 meters, in some sections of 15 - 18 meters.

Delta Square: 19 000 sq. Km.

Medium annual stock: \u003e 38 cubic cm.

Where leaks: The Volga originates in one of the most sublime parts of Valdai Plateau on the territory of the Tver region. She follows from the little Spring in the middle of the swamp lakes, not far from the village of Volkheerhovye. The coordinates of the source of 57 ° 15 'northern latitude and 2 ° 10' East longitude. The height of the source above sea level is 228 meters. The Volga flows through the entire central lowland of European Russia. The riverbed of the river willowfully, but the general direction of the flow is eastern. Kazan, approaching almost the farthests of the Urals, the river turns the river to the south. A truly mighty River Volga becomes only after the kama inserted into it. Samara Volga makes its way through a whole chain of hills and forms the so-called Samara bows. Not far from Volgograd Volga comes closer to another mighty river - Don. Here the river again makes turn and flows in the southeast direction until it flows into the Caspian Sea. At the mouth of the Volga forms an extensive delta and divides the set of sleeves.

River Mode, Food: Most of the water comes from groundwater and to a lesser extent the power occurs due to precipitation.

Freezing: The Volga ice is covered in late October - early November and remains under it until the end of April - mid-March.

Flows: About 200 tributaries fall into the Volga. The largest of which are Kama and Oka, as well as smaller robies such as: Unzha, Kergenets, Sura, Tver, Major and others.
Until now, it is not yet possible to assume that Kama flows into the Volga. Since according to the rules of hydrography, it turns out that everything is exactly the opposite, and this Volga must fall into the kama. Since Kama is older, her pool has more and tributaries too.

Direction of flow to the most part of the river from north to south. Between the tributaries of the eye and Kama - the Volga has a predominantly latitious current.
Over the centuries, the Volga served people, a source of pure water, fish, energy, transport artery. But today she is in danger, the human activity pollutes it and threatens the catastrophe.
Favorable geographical position The rivers and activities of a person on the construction of the channels turned the Volga to the largest transport artery. In addition to the Caspian Sea, it is connected with 4 seas: Baltic, White, Black and Azov. Its waters are irrigated by fields, and its hydroelectric power plants provide electricity whole cities and largest enterprises. However, intensive economic use led to the pollution of the Volga with industrial and agricultural waste. Huge territories were flooded in the construction of dams.

Environmentalists say that the environmental situation is critical and the possibilities of the river to self-cleaning are exhausted. Blue-green algae capture more and more territories every year, fish mutations are observed. The Volga is called one of the most dirtiest rivers of the world. Ecologists may love to dramatize, but if it becomes too late, it will be much worse. In any case, there are problems. Therefore, the protection of the river is very important now.

The river drains the territory of the Eastern European Plain. Square with altitudes below 200 m occupy 80% of the basin surface. On 5% of the height of the height reach 600-700 m (maximum up to 1500 m). Surface Caspian lowland It is below the level of the World Ocean (markers -27.8 m and above).

In the river basin, there are fields of oil, gas, coal, potash salts, etc. It produces 60 million tons of oil; Large deposits are operated natural Gas. Coal is mined in Tula, Kaluga, Chelyabinsk, Sverdlovsk regions, Republic of Bashkortostan. In the area of \u200b\u200bSolikamsk, the deposits of potash salts are being developed, in the Lower Volga region - the table salt (Lake Baskunchak and Elton).

The Volga's pool is located in the zone of moderately continental climate. The air temperature is increasing from north to south. average temperature January varies in the range -4 ... -8 ° C (south-west) and -16 ... -20 ° C (northeast pool). The average temperatures of July are reduced from the south-south-west (24 ° C) to the North-North-East (16 ° C). In the north of the Volga basin, 500-600 mm of precipitation falls annually, on the Western slopes of the Ural Mountains - 800 mm. The layer of precipitation in the southern pilot and on the Caspian lowland is 180-200 mm. The evaporation layer decreases from 500 (south-west) to 200-250 mm in the northeast. The southern part of the pool is located in the arid climate zone.

Most part of the Volga basin is busy coniferous forests and turf-podzolic soils. European-type souder-handed forests stretch out a strip from Valdai to the northern part of the pool of the Kama. Separate arrays of broadly oak and lipovo-oak forests are preserved in the areas of Samara Luke, a high voltage and the Western Urals. On the slopes of the Urals, the distribution of soil-vegetation cover is obeying the law of high-altitude. Steppe vegetation and chestnut soils are characteristic of the middle and southern parts of the Volga basin. Desert vegetation is developed within the Caspian lowland. Azonal vegetation is characteristic of the Volga delta. Within the Volga basin there are 23 reserves and 18 national parks.

Pool Volga is the most developed region of Russia. Within its limits, there are more than 30 constituent entities of the Russian Federation, more than 40% of the country's population lives, about 45% of its industrial and 50% agricultural production is concentrated. Here are seven cities with a population of more than 1 million people, including Moscow - the capital of Russia. In the north of the pool, the population density is reduced; In the middle part of the pool, the maximum reaches. The density of the population is large and in its lower part.

In the regions of the region, more than 90% of the country's cargo and passenger cars are produced, mountain, metallurgical and chemical equipment are produced, the car building, the production of heavy machines, construction and road machines, tractor construction is developed. In the northwest of the pool are enterprises of energy and electrical engineering, maritime shipbuilding, car buildings, machine-tooling, production industrial equipment. According to the release of the chemical industry, the enterprise of the region occupy a leading place in the Russian Federation. The Volga basin produces 62% of the products of the country's light industry. The Volga pool occupies a leading place in the country for the production of business wood.

About 50% of the agricultural production of the Russian Federation is concentrated here. The main branch of production in the Central Economic Area (ER) is animal husbandry and crop production. Novgorod region specializes in growing flax. In the Volga-Vyatka ER developed crop production (grain, flax). In the Central Black Ear ER, the winter wheat is grown, rye, sugar bed, sunflower, gardening and vegetable growing developed. Grain and vegetable cultures are grown in Volga ER, animal husbandry developed. On average and partially in the Lower Volga region, large areas are engaged in crops of industrial crops. Bahchoeva and gardening developed. Ural ER ranks second in Russia on animal husbandry and fourth on crop production.

In the upper flow of the Volga (to the city of the old man), a winding or relatively straight line of the river is located in the canyon depth of 30-40 m. The shores and the bottom are folded by boulders and loam, below Rzhev - limestones. From the old man to the mouth of the r. Selulation of the valley of the river is obvious, its slopes of the field and wetched. When crossing the Vyshnevotsk, the river river flows in a relatively deep valley with steep slopes, folded loams and sands. The embedded radiation alternate here with the areas of the river with a narrow bilateral floodplain having relatively rectilinear outlines. Damage deposits are sandy-pebble. The channel has a width of up to 50 m, steadily. On the Volga region between the mouth of the r. Selulation and the city of Tver Width of the river increases from 40 to 200 m.

On the plot between the Tver and the Rybinsky River are substrued by dams of Ivankovsky, Uglich and Rybinsky reservoirs. Below Rybinsk, the riverbed and the floodplain of the river are under the waters of Gorky (Nizhny Novgorod) reservoir. In the lower beast of the Rybinsky reservoir, the bottom of the bottom is an average of 3.5 cm / year, and the rate of recession of the shore is 3 m / year.

On average, the Volga flows along the Volga Hills. The right bank of the river and the Cheboksar reservoir is high and cool. There are frequent landslides and collaps. They contribute to the wave recycling shores. The left subsidence is basically low and sandy. Below, the hydrological state of the river is determined by the operating conditions of Kuibyshevsky, and below the flow of Saratov and Volgograd reservoirs. In the area of \u200b\u200bthe Volgograd Reservoir Dam from the Volga, the Left-Bank Called Sleeve - Akhtuba (Length is 537 km). Between the Volga and Akhtuba there is an extensive space (width to 40 km), separated by numerous ducts and storms (Volga-Akhtubinskaya floodplain). Below Volgograd Volga flows along the right indigenous shore. Up to 40% of the river length from Volgograd to Astrakhan is actively blurred by the flow. The average smoke rates of floodplain shores decrease downstream from 15.2 to 10-12 m / year. Lower Volga is the prevalence zone of sections of a sand branched and winding bed.

The mouth of the Volga starts 54 km north of Astrakhan; Includes a delta (area of \u200b\u200b13900 km 2) and a wellhead seaside (28000 km 2). The largest delta sleeves: Buzan, Bold, Kizan (Kamizyak), Bakhtemir. Akhtuba flows into Buzan. Below the source of Buzana is the Volga Petrifier (built in 1966-1973), designed to increase the runoff in the eastern part of the delta. The mouth seaside is engaged in river water. The shallow seaside crosses 28 fisheries and three shipping channels. Volga-Caspian Channel (undergoing Bakhtemir's sleeve), combines the Volga and the Caspian Sea.

The average coherent water consumption below the Uppervolzh reservoir is 29 m 3 / s; Rybinsky reservoir - 969 m 3 / s; Ur Nizhny Novgorod - 1530 m 3 / s; In Saratov - 7570 m 3 / s, in Volgograd - 8060 m 3 / s. The average miniature water consumption at the top of the delta (1961-2010) is 7870 m 3 / s, and water flow is equal to 248.385 km 3 / year. The mid-year precipitation layer is 660 mm, a layer of evaporation - 480 mm, layer of flow - 180 mm. The bulk of the flow is formed in the forest area of \u200b\u200bthe Volga basin. The melting of snow gives 60%, unloading groundwater - 30%, rain loss - 10% of the annual flow. The water flow module increases from the south to the north. The maximum values \u200b\u200bof the runoff module exceed 10 l / (C ∙ km 2) (Valdai hill, Western Ural); On the Volga Hills, it is 2-5 l / (C ∙ km 2), on the Caspian lowland does not exceed 0.2 l / (C ∙ km 2).

The Volga refers to rivers with the Eastern European type of water regime: with spring flood (April-June), low summer and winter land and autumn rain floods (October). The maximum cost of water takes place 5-15 days after the start of the flood. The duration of the flood is an average of 72 days. Maximum water consumption y with. Yeltsi is 748 m 3 / s; At the city of Nizhny Novgorod - 7750, at the top of the Volga delta (after creating a cascade of reservoirs) - did not exceed 35,000 m 3 / s. After creating the Volga-Kamsky cascade, the reservoir of the flood in the lower times of the Volga began to begin at the end of the second decade of April. Maximum flow, on the contrary, is observed for about two weeks earlier. The duration of the flood decreased from 116 to 71 days, significantly decreased and the range of intra-divine changes in water levels. Summer airway usually begins in June. Minimum water consumption y with. Yeltsi is 6.10 m 3 / s, in the city of Nizhny Novgorod - 115 m 3 / s. The share of interventic drains reaches 28% annual flow.

The average annual turbidity of water in the upper reaches of the Volga varies from 10 to 140 g / m 3; In the basin of the River Oki and Sura, the upper and middle part of the pool of Kama, the left-bank tributaries of white and the Volga - from 100 to 250 g / m 3. The greatest turbidity is characteristic of spring flood, the smallest - winter period. The creation of reservoirs led to a significant decrease in the turbidity and drainage of weighted nans. At the top of the Delta, the stock of weighted nansions is equal to 6.7 million tons / year (1961-2006).

Volga water belongs to the bicarbonate class and the calcium group. Mineralization of water in the upper flow of the Volga in the period of elevated flow does not exceed 100 mg / l. Downstream of the river, it increases to 180-200 mg / l. Before the condense of Okey, the mineralization of the water of the Volga varies in the range from 80 to 100 mg / l. In the area of \u200b\u200bKazan, mineralization during the snowmag is 100-200 mg / l, and below the mouth of the kama - about 140 mg / l. The maintenance of dissolved mineral substances in the water in water increases by 2-2.5 times. In terms of quality, water in the upper reaches of the Volga corresponds to moderately polluted rivers. In the Kuibyshev reservoir and below Volgograd, Volzhka water remains moderately polluted or contaminated.

The water fence from the Volga is about 26 km 3 / year. Intradinary water consumption close to 10 km 3 / year. The maximum water consumption is characteristic of the Astrakhan, Moscow, Nizhny Novgorod and Samara regions, Perm Territory. For provision drinking water The population of Moscow and the Moscow region is spent to 33% of the useful volume of the water of the Ivankovsky reservoir. From the Saratov reservoir, water is taken to supply a number of industrial facilities. On irrigation, the lands are taken from Kuibyshev, Saratov and Volgograd reservoirs.

Local shipping on the Volga is carried out everywhere below Tver. In the Volga basin, about 6 million tons of cargo is transported annually. In terms of transported goods on river transport, building materials prevail (60%). The largest river ports of the Volga basin: Moscow, Volgograd, Nizhny Novgorod, Yaroslavl, Perm, Astrakhan, Kazan, etc. In 2008, 520 thousand passengers took advantage of the services of the Volzhsky shipping company.

HPP of the Volga-Kamsky Cascade provides a large amount of electricity. Their total installed capacity is 8013 MW, and the average annual electricity generation is 31.6 billion kWh. The greatest installed capacity has the Volga HPP.

In the Volga inhabit about 70 species of fish, Of these, 40 commercial (vobla, herring, bream, pike perch, sazan, catfish, pike, core, sterlet, etc.).

N.I. Alekseevsky, M.M. Antonova

The main tributaries of the Volga (large and medium rivers)

With her "Rostov Mountains" and " sea coast Belarus ", on with menu is rumbling even more than a cheerful generation.

According to the results of the 2014 survey, it is confidently to say where the Volga flows, less than 60% of students of the Faculty of Journalism of Moscow State University were able to confidently. Students went over the options from Azov and black to the Northern and Baltic seas, in the Higher School of Economics suggested that the Volga flows into Baikal, OKU, the Pacific Ocean, and Moscow State University - in Moscow River, Yenisei, Ob. Some students decided that Volga did not fall anywhere. "

A total of 151 student Zhurfak MSU, 84 student Higher School Economy and 35 MGIMO students approximately equal number from all courses. Options for answers to students were not offered. Candidates were chosen randomly. Not a single student could answer all questions, 15 people could not answer any other question. You can check yourself after passing a simple test created on the basis of questions specified by students.

Contemporary the capital truth "Volga flows into the Caspian Sea" It is enough to know dla in total development. But those who want to figure out in history, it is necessary to keep in mind that this statement is essentially incorrect and to begin to understand the hydrological concepts.

FirstlyIt would be more correct to talk about the lifting river to the Caspian lake, because the seas are called parts of the World Ocean, and the Caspian Sea is a light-minded lake that has no connection to the world ocean and is called the sea by tradition apparently due to salt water and large sizes.

In other words, the River Pool Volga with the Caspian Sea-Lake isiNTERCONTINAL WATER WATER SYSTEM, FULLY INCELATED WITH OWN OCEAN. And this circumstance must be taken into account when studying the history of civilization, which is distributed mainly by seas and waterways.

For example, only three "entry points" in the Volga pool from different seas to be understood by their historical significance.

1. From the Baltic Sea, the first way on the rivers of Neva - Volkhov - Msta - Tereks, that is, the cities of Petersburg-great Novgorod - Tver. That is why here, and not somewhere else and was founded by the capital Russian Empire - Petersburg.

2. From the Black Sea along the Dnieper through the island of Hortiets (the base of the Zaporizhzhya Cossacks) and Kiev in the top of the Dnipro is the iconic "key city" Smolensk, then on the influx of Dnipro, the nodal city of Vyazma, from where it was possible to get into the upper places of the Oka and Volga pools.

3. From Azov Sea On Don, then in the influx of Tsiml (on the site of this river now the Tsimlyan reservoir) and the wolf to the Volga near the modern Volgograd. TOanal Volga-Don approximately corresponding to B.introduced by land waist and not at all by chance that it was there in the settlement of Dubok there was an administrative center of the Volga Cossacks, and not in the area of \u200b\u200bthe mouth of the river as all the other river Cossacks. Yes, yes, that's the way, each Cossack army initially controlled his river, the Cossacks generally initially waterfowl and only at the turn of 18-19 centuries moved to the horses.

SecondlyThe Caspian Sea Lake is not a Volga, but Kama. According to one of the main hydrological criteria - full-breeding, when the Volga merger, the last one is more complete + an additional criterion for the direct channel at the confluence of the merger, the Volga must be considered the influx of Kama, and not vice versa and then it is exactly that Kama flows into the Caspian Sea. Therefore, the ancient authors are not mistaken at all when they write that the RA River (Volga) flows with Rhypsian / Ripeye(Ural) Mountains.

River basins can be compared with trees that are closed by crowns. Like trees on the trunks, all rivers are definitely identifiable from the mouth, and then up the river for transport purposes need to be determined by the main watercourse, which is not always obvious.

For example, in the fusion site of the Volga with the latter, the latter was full and could be considered the main waterclock in this criterion, in this case it would be that Volga flows into OKU. But in this place the Volga straight channel and with approximately equal visual assessments of the fullness, she wins the right to be called the main watercourse.

In other words, the name of the river used to spread on the watercourses ranging from the mouth and up, against the flow, based on the practical goals of shipping. In the 19th century, this principle was changed to the opposite, assigning "one of the branches of the crown of the tree" the source of the river is simpler, but does not have any practical meaning, shipping distances in many places are still counted from the mouth of the rivers.

So the answer to inpoll "Where does the Volga fall?" Most considers it well-known, primitive only because ofoverround view on the river from top to bottom, from the source to the mouth and Creation of cleardefinitions of the main watercourse.

This mighty water flow flows through the extensive territories of the European part of Russia and flows into the Caspian Sea. This is the largest river in Europe for the length of the river, and it has the right to be considered a national symbol of Russia.

This is the Volga River, in which many largest cities are located in the pool. russian state, among whom his capital is Moscow.

The article presents some information about the Volga River: width and depth, length and features of the flow.

Main characteristics

The overall length of the river from the source to the mouth is 3692 km. Officially, not counting the plots of reservoirs, the length of the Volga River is considered to be 3530 kilometers.

The area of \u200b\u200bthe water basin is 100380 square kilometers, which is 1/3 of the area of \u200b\u200bthe European territory of Russia.

What is the depth of the Volga? In the article, try to find an answer to this question. But first consider the path of the river from the source to the mouth. She starts his way on Valdai Hills, in the Tver region (Ostashkovsky district). Near the village Volgoverhhovye from under the ground beat the keys, one of which is the source of the Great Russian River (the height of the UR. Sea is about 228 meters). The spring is fenced with a chapel, to come to which you can bridge. From a small reservoir, which flows all nearby springs, flows the handle with a width of about 1 meter and a depth of no more than 30 cm.

Beginning of the Great River

The conditionally river is divided into 3 sections: upper, middle and lower Volga. First large city On the way of a huge water flow is Rzhev. The distance to it from the source is 200 km. The next large settlement is the old city of Tver (population - more than 400 thousand people). There is a 120 kilometers long, Ivankov reservoir. The Volga Depth in the area increases to 23 meters. It is a Uglich reservoir (146 km - length, 5 meters - depth). A little north of Rybinsk is the Rybinsk reservoir, where the northernmost point of the Volga is located. After this mark, the river turns to the southeast (before that it flows in the northeast direction).

In the area of \u200b\u200bthe Gorky reservoir on the banks of the river, Yaroslavl, Kineshma, Kostroma will spread out. Above Nizhny Novgorod is the district center of Gorodets. The Nizhny Novgorod HPP is constructed here, which forms a Gorky reservoir, the length of which is 427 km.

The depth of the Volga in this area is on average equal to 1.8-2.1 meters.

This plot begins after the combination of the Volga with the Okoy, which is its largest right influx. Its length is 1499 kilometers. She flows into the Volga in the area of \u200b\u200bNizhny Novgorod.

The Volga River, having accepted the water of Oka, becomes wider and sent to the east. It flows along the northern territory of the Volga Hills. Cheboksary's city is blocked by Cheboksary HPP, forming the reservoir of the same name, the length of which in length is 341 kilometers, and the width is 16 kilometers. The maximum depth of the Volga in the area is 35 meters, and the average - 5 m. Next the course of the river is sent to the southeast, and Kazan turns to the south.

Lower Volga

A truly great and mighty Volga becomes the kama - the largest left bilge into it. The length of this river is 1805 km, and the Volga is superior in many parameters. So why not she falls into the Caspian Sea? And this is connected with the established historical traditions and names.

After reuniting these two the largest rivers The lower flow of the Volga begins. Next, she moves all the time to the south, in the direction of the Caspian Sea. On the shores of this part of the river, such cities like Ulyanovsk, Samara, Tolyatti, Saratov and Volgograd are located. The cities of Samara and Tolyatti formed an exhaustion (Samara Luka), directed to the east. Here the flow of water envelopes Togliatti mountains. Located here (slightly higher in the flow) the largest Kuibyshev reservoir on the Volga, which in the area ranks third in the world. Its length is 500 km, width - 40 km. The depth of the Volga on this area is 8 meters.

Features Delta River

At the Caspian Sea, the length of the river delta is approximately 160 km. In width, it reaches 40 km. The Delta includes approximately 500 channels and small rivers. It is believed that the mouth of this great River is the largest in all of Europe. It should be noted that in these places you can meet the most unique representatives of both plant and the animal world. For example, here you can find flamingos and pelicans, and you can also see the flowering lotus.

The maximum depth of the Volga River in the delta by different information is 2.5 meters. The minimum depth is about 1.7 meters.

In terms of its Delta, Volga surpasses Terek, Kuban, Rhine and Maas. It is important to note that there were once important trading routes that bind the lower Volga with the Persia and other Arab States. Inhabited these places of the tribes of Polovtsy and Khazarov. According to some reports, in the XIII century, in these places, the Tatar settlement appeared for the first time, called Ashtarhan, who became the beginning of Astrakhan.

Keywords: Parameters of the Volga River, Depth, Extension, Details, Volga River, Expite Volga, Gorodets, Medium Volga